Like other major valleys or gaps in the Chilterns that run approximately North-South, the Bradenham valley was predominantly formed during Pleistocene Epoch (the Ice Ages), between 2.5 million and 10,000 years ago. Like most other Chiltern valleys, it is now a dry valley because the underlying chalk is permeable to water. During the Ice Age, in permafrost conditions, water could not pass through the frozen ground. Seasonal thawing, particularly of the ice sheets to the north, would have released large amounts of water, which would have cut down into the chalk to create the present “fossil” valley.
nationaltrust.org.uk/chilterns-countryside/trails/bradenham-beech-woods-and-bunkers-trail

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Elevation 210 m

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Location: Bradenham, Wycombe, Buckinghamshire, South East England, England, United Kingdom

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Bradenham Valley

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